TY - JOUR
T1 - Stabilized high-order Galerkin methods based on a parameter-free dynamic SGS model for LES
AU - Marras, Simone
AU - Nazarov, Murtazo
AU - Giraldo, Francis X.
N1 - Funding Information:
The authors are thankful to the editor of this paper, Prof. Smolarkiewicz and to two anonymous reviewers whose comments helped improve the document. The discussions with and inputs by Prof. Lucas Wilcox (NPS), Dr. Matias Avila (BSC-CNS), and Dr. James F. Kelly (Exa Corp.) are also very much appreciated. The first and third authors acknowledge the support of the Office of Naval Research through program element PE-0602435N , the National Science Foundation (Division of Mathematical Sciences) through program element 121670 , and the Air Force Office of Scientific Research through the Computational Mathematics program. The work of the first author was supported by the National Academies via a National Research Council fellowship.
Publisher Copyright:
© 2015 Elsevier Inc.
PY - 2015/11/15
Y1 - 2015/11/15
N2 - The high order spectral element approximation of the Euler equations is stabilized via a dynamic sub-grid scale model (Dyn-SGS). This model was originally designed for linear finite elements to solve compressible flows at large Mach numbers. We extend its application to high-order spectral elements to solve the Euler equations of low Mach number stratified flows. The major justification of this work is twofold: stabilization and large eddy simulation are achieved via one scheme only.Because the diffusion coefficients of the regularization stresses obtained via Dyn-SGS are residual-based, the effect of the artificial diffusion is minimal in the regions where the solution is smooth. The direct consequence is that the nominal convergence rate of the high-order solution of smooth problems is not degraded. To our knowledge, this is the first application in atmospheric modeling of a spectral element model stabilized by an eddy viscosity scheme that, by construction, may fulfill stabilization requirements, can model turbulence via LES, and is completely free of a user-tunable parameter.From its derivation, it will be immediately clear that Dyn-SGS is independent of the numerical method; it could be implemented in a discontinuous Galerkin, finite volume, or other environments alike. Preliminary discontinuous Galerkin results are reported as well. The straightforward extension to non-linear scalar problems is also described. A suite of 1D, 2D, and 3D test cases is used to assess the method, with some comparison against the results obtained with the most known Lilly-Smagorinsky SGS model.
AB - The high order spectral element approximation of the Euler equations is stabilized via a dynamic sub-grid scale model (Dyn-SGS). This model was originally designed for linear finite elements to solve compressible flows at large Mach numbers. We extend its application to high-order spectral elements to solve the Euler equations of low Mach number stratified flows. The major justification of this work is twofold: stabilization and large eddy simulation are achieved via one scheme only.Because the diffusion coefficients of the regularization stresses obtained via Dyn-SGS are residual-based, the effect of the artificial diffusion is minimal in the regions where the solution is smooth. The direct consequence is that the nominal convergence rate of the high-order solution of smooth problems is not degraded. To our knowledge, this is the first application in atmospheric modeling of a spectral element model stabilized by an eddy viscosity scheme that, by construction, may fulfill stabilization requirements, can model turbulence via LES, and is completely free of a user-tunable parameter.From its derivation, it will be immediately clear that Dyn-SGS is independent of the numerical method; it could be implemented in a discontinuous Galerkin, finite volume, or other environments alike. Preliminary discontinuous Galerkin results are reported as well. The straightforward extension to non-linear scalar problems is also described. A suite of 1D, 2D, and 3D test cases is used to assess the method, with some comparison against the results obtained with the most known Lilly-Smagorinsky SGS model.
KW - Adaptive dissipation
KW - Discontinuous Galerkin
KW - Dynamic SGS model
KW - LES
KW - Large eddy simulation
KW - Localized artificial viscosity
KW - Low Mach number
KW - Non-hydrostatic atmospheric flows
KW - Spectral element method
KW - Stratified flows
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U2 - 10.1016/j.jcp.2015.07.034
DO - 10.1016/j.jcp.2015.07.034
M3 - Article
AN - SCOPUS:84940181612
SN - 0021-9991
VL - 301
SP - 77
EP - 101
JO - Journal of Computational Physics
JF - Journal of Computational Physics
ER -